Phase equilibria in the H2O–CO2 system between 250–330K and 0–1.7GPa: Stability of the CO2 hydrates and H2O-ice VI at CO2 saturation

Autor: C. Taffin, Yann Morizet, A. Oancea, Olivier Grasset, Erwan Le Menn, Mathieu Choukroun, L. Bezacier, O. Bollengier, Guillaume Bellino, Gabriel Tobie

Publikováno v: Geochimica et Cosmochimica Acta
Geochimica et Cosmochimica Acta, 2013, 119, pp.322-339. ⟨10.1016/j.gca.2013.06.006⟩
Geochimica et Cosmochimica Acta, Elsevier, 2013, 119, pp.322-339. ⟨10.1016/j.gca.2013.06.006⟩

Although carbon dioxide is of interest in planetary science, few studies have been devoted so far to the H2O–CO2 system at pressures and temperatures relevant to planetary interiors, especially of the icy moons of the giant planets. In this study,

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f5d69a04c615be6fb607c18f9717fa35
https://doi.org/10.1016/j.gca.2013.06.006